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E = o T 4
| Date post: | 04-Jan-2016 |
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E = o T4
Variables List Power = Irradiance * Area
Variables List mass = (2897 m K)/T
E (at latitude a) = (1378.5 W m-
2)(sin a)
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Albedo = (Upwelling) / (Downwelling radiaiton)
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Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 8 - Infrared Water Vapor Imagery for 11 March 2000
at 1745 UTC (11:45 AM CST)
Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 12 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
Figure 13 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 8 - Infrared Water Vapor Imagery for 11 March 2000
at 1745 UTC (11:45 AM CST)
Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 8 - Infrared Water Vapor Imagery for 11 March 2000
at 1745 UTC (11:45 AM CST)
Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
Figure 12 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
Figure 13 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
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